Bulletin of the Seismological Society of America; August 1995; v. 85; no. 4;
p. 1244-1248
© 1995 Seismological Society of America
Propagation of high-frequency (4- to 50-Hz) P waves in the northeastern United States
Eric P. Chael,
Patrick J. Leahy,
Jerry A. Carter,
Noël Barstow and
Paul W. Pomeroy
Sandia National Laboratories, MS 0655, Albuquerque, New Mexico 87185
SAIC, 1300 North 17th St., Arlington, Virginia 22209
Lamont-Doherty Earth Observatory of Columbia University, Palisades, New York 10964
, POB 224, Stone Ridge, New York 10964
Abstract
We have measured the decay rate of high-frequency (4- to 50-Hz) P waves in the northeastern United States. We analyzed signals from 28 explosions of a 1988 USGS/AFGL/GSC refraction survey recorded at distances between 30 and 400 km. Over this range, the decay rate steadily increases from
2 at 10 Hz to
4 at 45 Hz. If one assumes geometric spreading of
1.3, then the remaining decay is consistent with a nearly frequency-independent Q of about 1000. The results provide a useful parameterization for predicting P-wave spectra at near-regional ranges.
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